Jb. Milford et al., TOTAL REACTIVE NITROGEN (NO(Y)) AS AN INDICATOR OF THE SENSITIVITY OFOZONE TO REDUCTIONS IN HYDROCARBON AND NOX EMISSIONS, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 99(D2), 1994, pp. 3533-3542
For areas in the United States not meeting the federal air quality sta
ndard for ozone, an issue of continuing controversy is the emphasis to
be placed on controlling nitrogen oxides (NO(x)) in addition to emiss
ions of reactive organic gases (ROG). To assess conditions under which
ROG or NO(x) controls would be most effective, we have analyzed predi
ctions from four studies that represent different locations and meteor
ological conditions, distinct chemical inputs, e.g., with or without s
ignificant biogenic emissions, and different air quality models. A con
sistent association is found between the sensitivity of ozone to reduc
tions in ROG versus NO(x) emissions and the simulated total reactive n
itrogen (NO(y)) at the time and place of peak ozone. In the studies ex
amined, ozone was predicted to be reduced most effectively by ROG cont
rols at locations where NO(y) concentrations exceeded a threshhold val
ue falling in the range of 10 to 25 ppb, whereas NO(x) controls were p
redicted to be more effective where NO(y) concentrations were below th
at threshhold. The NO(y) level explains much of the difference in ozon
e sensitivity at different locations and provides a basis for comparis
on of predicted sensitivity from different models. In contrast, the mo
rning concentration ratio of ROG to NO(x) that has been used in the pa
st is a less reliable indicator Of 03 sensitivity. Measurement of NO(y
) concentrations along with ozone would assist in empirical testing of
model predictions of responses to emission reductions.